Abstract

Abstract. Land use and cover have been significantly changed all around the world during the last decade. In particular, the Grain for Green (GG) program has resulted in significant changes in regional land use and cover, especially in China. Land use and cover change (LULCC) may lead to changes in regional climate. In this study, we take the Yangtze River basin as a case study and analyze the impacts of LULCC and reforestation on summer rainfall amounts and extremes based on the Weather Research and Forecasting model. Firstly, two observed land use and cover scenarios (1990 and 2010) were chosen to investigate the impacts of LULCC on summer rainfall during the last decade. Secondly, two hypothetical reforestation scenarios (i.e., scenarios of 20 % and 50 % cropland changed to forest) were taken based on the control year of 2010 to test the sensitivity of summer rainfall (amounts and extremes) to reforestation. The results showed that average summer rainfall and extreme summer daily rainfall decreased in the Yangtze River basin between 1990 and 2010 due to LULCC. Reforestation could increase summer rainfall amount and extremes, and the effects were more pronounced in populated areas than over the whole basin. Moreover, the effects of reforestation were influenced by the reforestation proportion. In addition, the summer rainfall increased less conversely, with the transform proportion of cropland to forest increased from 20 % to 50 %. By analyzing the changes in water vapor mixing ratio, upward moisture flux, and 10 m wind, it is suggested that this result might be caused by the horizontal transportation processes of moisture. Although a comprehensive assessment of the impacts of LULCC on summer rainfall amounts and extremes was conducted, further studies are needed to investigate the uncertainty better.

Highlights

  • Human activities intensify land use and land cover change (LULCC) all around the world

  • The negative biases are mainly observed in the southeastern Yangtze River basin (YRB), which were found in other studies (Zhang et al, 2017)

  • The positive biases are mainly observed in the upstream area where the altitudes are higher than 1200 m, while the negative biases are mainly observed in the midstream and downstream areas, with the maximum negative biases located in the southeastern YRB

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Summary

Introduction

Human activities intensify land use and land cover change (LULCC) all around the world. LULCC can influence climate through various geophysical processes, such as the water and heat flux between the land surface and the atmosphere, surface wind speed, and boundary layer turbulence. LULCC can affect regional climate significantly, which is a broad consensus reached by many studies. Wen et al (2013) found that land use changes in China could contribute to the warmest day temperature increases. Lin et al (2020) showed that urbanization tended to result in weak extreme rainfall events in urban agglomerations over coastal regions and intensifies the influences on those in central and western China Yu et al (2020) found that the recent greening in China has resulted in a country-averaged surface cooling of 0.11 ◦C. Lin et al (2020) showed that urbanization tended to result in weak extreme rainfall events in urban agglomerations over coastal regions and intensifies the influences on those in central and western China

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